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路易斯维尔海山链6400 - 7400万年前海底火成岩基底中的细菌丰度和多样性。

Bacterial abundance and diversity in 64-74 Ma subseafloor igneous basement from the Louisville Seamount Chain.

作者信息

Sylvan Jason B, Tully Benjamin J, Morono Yuki, Alt Jeffrey C, Grim Sharon L, Inagaki Fumio, Koppers Anthony A P, Edwards Katrina J

机构信息

Department of Biological Sciences University of Southern California Los Angeles California USA.

Present address: Department of Oceanography Texas A&M University College Station Texas USA.

出版信息

mLife. 2024 Dec 24;3(4):578-583. doi: 10.1002/mlf2.12148. eCollection 2024 Dec.

Abstract

The aquifer in the subseafloor igneous basement is a massive, continuous microbial substrate, yet sparingly little is known about life in this habitat. The work to date has focused largely on describing microbial diversity in the young basement (<10 Ma), where the basaltic crust is still porous and fluid flow through it is active. Here, we test the hypothesis that microbial life exists in subseafloor basement >65 Ma using samples collected from the Louisville Seamount Chain via seafloor drilling. Cell biomass was heterogeneous in nature, ranging from below detection to ~10 cells cm. Bacterial 16S rRNA genes from core samples and enrichment incubations are dominated by lineages putatively carrying out nitrogen, sulfur, and metal redox processes and hydrocarbon oxidation. Taken together, the data indicate that microbial life is indeed present in subseafloor igneous basement >65 Ma, which significantly expands the range of the subseafloor biosphere where microbial life is known to exist.

摘要

海底火成岩基底中的含水层是一个巨大且连续的微生物生存基质,但对于这个栖息地中的生命,我们知之甚少。迄今为止的研究主要集中在描述年轻基底(<10 Ma)中的微生物多样性,那里的玄武岩地壳仍然多孔,通过它的流体流动活跃。在这里,我们通过海底钻探从路易斯维尔海山链采集样本,来检验年龄大于65 Ma的海底基底中存在微生物生命的假设。细胞生物量在本质上是异质的,范围从低于检测限到约10个细胞/立方厘米。来自岩心样本和富集培养物的细菌16S rRNA基因主要由推测进行氮、硫和金属氧化还原过程以及碳氢化合物氧化的谱系主导。综合来看,数据表明微生物生命确实存在于年龄大于65 Ma的海底火成岩基底中,这显著扩大了已知存在微生物生命的海底生物圈范围。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/14cb/11685831/4e14c2972b91/MLF2-3-578-g001.jpg

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